FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W4212918881> ?p ?o ?g. }

• W4212918881 endingPage "110261" @default.
• W4212918881 startingPage "110261" @default.
• W4212918881 abstract "With petroleum exploration extending to deeper reservoirs, it becomes more and more difficult to find relatively high-quality reservoirs in heterogeneous sandstones. This research integrates fluid inclusion analysis, petrographic, mineralogical, and geochemical data to determine the origin of authigenic minerals, establish the porosity evolution model and discuss diagenetic effects on reservoir quality of the fourth member of the Upper Triassic Xujiahe Formation. The main rock types of studied sandstones are identified by thin-section, SEM and XRD analysis-feldspathic litharenites, litharenites, calcareous sandstone and chlorite-rich sandstone. Of the four types of sandstone, reservoir porosity of the chlorite-rich sandstone is generally the highest. Target sandstones have experienced complicated diagenetic histories including mechanical compaction, three stages of carbonate cementation, the dissolution of K-feldspar or rock fragments, three kinds of authigenic chlorite precipitation, and two stages of quartz precipitation. Two reaction pathways between K-feldspar and kaolinite were determined and limited dissolution was generated in the closed diagenetic system. Diagenetic sequence and porosity evolution suggest that the critical factors in reducing reservoir quality can be attributed to early intense compaction and widespread calcite cementation. The genesis of high-quality reservoirs among the various lithologies is different. In feldspathic litharenites and litharenites, the key factors for the development of relatively high-quality reservoirs is the acidic dissolution of K-feldspar and less cement being present in the rock. Because chlorite helps retain primary pores by inhibiting quartz overgrowths, almost all chlorite-rich sandstone are relatively high-quality reservoirs. In general, the reservoir quality of calcareous sandstone is poor unless fractures exist that can improve permeability. Determining the porosity evolution of various lithologies is an effective method to predict relatively high-quality reservoirs, which can provide a useful reference for deep petroleum exploration in other areas." @default.
• W4212918881 created "2022-02-24" @default.
• W4212918881 creator A5016354429 @default.
• W4212918881 creator A5047741511 @default.
• W4212918881 creator A5060711657 @default.
• W4212918881 creator A5073069692 @default.
• W4212918881 date "2022-05-01" @default.
• W4212918881 modified "2023-10-18" @default.
• W4212918881 title "The genesis of authigenic minerals and the porosity evolution of various lithologies and their implications for identifying high-quality reservoirs in the fourth member of Xujiahe Formation (Northeast-Sichuan Basin, China)" @default.
• W4212918881 cites W1219489599 @default.
• W4212918881 cites W1849879787 @default.
• W4212918881 cites W1866526036 @default.
• W4212918881 cites W1969929637 @default.
• W4212918881 cites W1979819137 @default.
• W4212918881 cites W1986695085 @default.
• W4212918881 cites W2000555315 @default.
• W4212918881 cites W2009916340 @default.
• W4212918881 cites W2011307050 @default.
• W4212918881 cites W2015821388 @default.
• W4212918881 cites W2019199746 @default.
• W4212918881 cites W2023135402 @default.
• W4212918881 cites W2025227538 @default.
• W4212918881 cites W2031255046 @default.
• W4212918881 cites W2046028043 @default.
• W4212918881 cites W2060831061 @default.
• W4212918881 cites W2061342415 @default.
• W4212918881 cites W2062367556 @default.
• W4212918881 cites W2068097994 @default.
• W4212918881 cites W2082867601 @default.
• W4212918881 cites W2083432263 @default.
• W4212918881 cites W2100212219 @default.
• W4212918881 cites W2113601502 @default.
• W4212918881 cites W2130363357 @default.
• W4212918881 cites W2135598297 @default.
• W4212918881 cites W2145808114 @default.
• W4212918881 cites W2162910251 @default.
• W4212918881 cites W2526610389 @default.
• W4212918881 cites W2554923541 @default.
• W4212918881 cites W2554996062 @default.
• W4212918881 cites W2762023997 @default.
• W4212918881 cites W2789993861 @default.
• W4212918881 cites W2807735381 @default.
• W4212918881 cites W2883162410 @default.
• W4212918881 cites W2883197540 @default.
• W4212918881 cites W2886566032 @default.
• W4212918881 cites W2925242767 @default.
• W4212918881 cites W2955969880 @default.
• W4212918881 cites W2987182603 @default.
• W4212918881 cites W2996880800 @default.
• W4212918881 cites W3003921492 @default.
• W4212918881 cites W3004709584 @default.
• W4212918881 cites W3018605764 @default.
• W4212918881 cites W3022077580 @default.
• W4212918881 cites W3040050837 @default.
• W4212918881 cites W3045918942 @default.
• W4212918881 cites W3216617504 @default.
• W4212918881 cites W595389199 @default.
• W4212918881 doi "https://doi.org/10.1016/j.petrol.2022.110261" @default.
• W4212918881 hasPublicationYear "2022" @default.
• W4212918881 type Work @default.
• W4212918881 citedByCount "4" @default.
• W4212918881 countsByYear W42129188812022 @default.
• W4212918881 countsByYear W42129188812023 @default.
• W4212918881 crossrefType "journal-article" @default.
• W4212918881 hasAuthorship W4212918881A5016354429 @default.
• W4212918881 hasAuthorship W4212918881A5047741511 @default.
• W4212918881 hasAuthorship W4212918881A5060711657 @default.
• W4212918881 hasAuthorship W4212918881A5073069692 @default.
• W4212918881 hasConcept C115393850 @default.
• W4212918881 hasConcept C122792734 @default.
• W4212918881 hasConcept C127313418 @default.
• W4212918881 hasConcept C130452526 @default.
• W4212918881 hasConcept C151730666 @default.
• W4212918881 hasConcept C166957645 @default.
• W4212918881 hasConcept C17409809 @default.
• W4212918881 hasConcept C191897082 @default.
• W4212918881 hasConcept C192562407 @default.
• W4212918881 hasConcept C199289684 @default.
• W4212918881 hasConcept C2777844515 @default.
• W4212918881 hasConcept C2778520076 @default.
• W4212918881 hasConcept C2778572594 @default.
• W4212918881 hasConcept C2779086746 @default.
• W4212918881 hasConcept C2779870107 @default.
• W4212918881 hasConcept C2780191791 @default.
• W4212918881 hasConcept C2780659211 @default.
• W4212918881 hasConcept C523993062 @default.
• W4212918881 hasConcept C94556721 @default.
• W4212918881 hasConcept C95457728 @default.
• W4212918881 hasConceptScore W4212918881C115393850 @default.
• W4212918881 hasConceptScore W4212918881C122792734 @default.
• W4212918881 hasConceptScore W4212918881C127313418 @default.
• W4212918881 hasConceptScore W4212918881C130452526 @default.
• W4212918881 hasConceptScore W4212918881C151730666 @default.
• W4212918881 hasConceptScore W4212918881C166957645 @default.
• W4212918881 hasConceptScore W4212918881C17409809 @default.
• W4212918881 hasConceptScore W4212918881C191897082 @default.
• W4212918881 hasConceptScore W4212918881C192562407 @default.
• W4212918881 hasConceptScore W4212918881C199289684 @default.

• next